摘要
东北地区主要土壤有效硅平均含量为392ms/ks,含量范围在97.0-897.4mg/kg之间,且黑土>褐土>草甸土>棕壤>白浆土。大部分黑土和褐土属于较高水平,而白浆土、草甸土和棕壤偏低。分析土壤有效硅与土壤理化性状的相关关系,得知有效硅含量与土壤的pH及粘粒含量达极显著和显著水平,此外,有效硅含量还与成土过程有关。
The average amount of available silicon of main soils in the Northeast Region is 392mg/Kg,range from 97.0 to 897.4mg/Kg,and Black Soil>Cinnamon soil>Meadow soil>Brown earth>Albic soil.The level of available silicon is higher in Black soil and Cinnamon soil, but lower in Albic soil、Meadow soil and Brown earth.There is a correlation between available silicon content and pH value or clay content of soils,except it is influenced by pedogensis.
出处
《黑龙江八一农垦大学学报》
1996年第4期42-45,共4页
journal of heilongjiang bayi agricultural university
关键词
土壤
硅
土壤理化性状
Available silicon
Physical and chemical properties of soil Pedogenesis